Journal article Open Access

# Analysis of the Marshall Islands Fireball of February 1, 1994

Tagliaferri, E.; Spalding, R.; Jacobs, C.; Ceplecha, Z.

### Citation Style Language JSON Export

{
"DOI": "10.1007/bf00671553",
"author": [
{
"family": "Tagliaferri, E."
},
{
"family": "Spalding, R."
},
{
"family": "Jacobs, C."
},
{
"family": "Ceplecha, Z."
}
],
"issued": {
"date-parts": [
[
1995,
1,
1
]
]
},
"abstract": "On February 1, 1994, a large meteoroid impacted over the Pacific Ocean at 2.6\u00b0 N, 164.1\u00b0 E. The impact was observed by space based IR sensors operated by the US Department of Defense and by visible wavelength sensors operated by the US Department of Energy. During entry the object broke into several pieces, one of which detonated at 34 km and another at 21 km altitude. The entry velocity of the object is estimated to be 24\u201325 km/sec. Based on the visible wavelength data, the integrated intensity of the radiated energy of the fireball was approximately 1.3 \u00d7 1013 joules. Assuming a 6000 K black body and a 30% efficiency for the conversion of the kinetic energy of the body into visible light, we estimate the mass of the body to be between 1.6\u00d7105 kg and 4.4\u00d7106 kg, and to have a diameter of between 4.4 and 13.5 meters. The object entered at a 45\u00b0 angle, traveling on a heading of approximately 300\u00b0, i.e. from the southeast to the northwest. Calculations using a gross-fragmentation model indicate that the body was most likely a stony object larger than 10 m with an Apollo orbit prior to impact.",
"title": "Analysis of the Marshall Islands Fireball of February 1, 1994",
"type": "article-journal",
"id": "1232448"
}
304
119
views